DOCSLIB.ORG

Kasmere Lake NTS

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

Manitoba Geological Survey B.G.C.M. Series Kasmere Lake, NTS 64N, 1:250 000 MARGINAL NOTES LEGEND The Kasmere Lake map area (NTS 64N) lies on the south and east flanks of the Hearne Province, part of the The Wollaston Domain and Seal River Domain share a common lithostratigraphy and metamorphic history. MUDJATIK DOMAIN SEAL RIVER DOMAIN Archean Rae-Hearne craton. The Snowbird Shear Zone divides the Rae-Hearne craton into the Rae Province Wollaston Group paragneiss unconformably overlies Archean granitoid rocks and possibly Archean volcanic Proterozoic Proterozoic to the west and the Hearne Province to the east (Hoffman, 1990). The Archean continental crust of the Hearne and sedimentary-derived gneiss. The Wollaston Domain is a northeast-trending fold belt with minor Hudsonian O O 0 102 O 100 0 0 0 Province is overlain by Paleoproterozoic cover rocks and, together with the cover rocks, has undergone varying plutonism, whereas the Seal River Domain exhibits an early, easterly trending, open fold set locally overprinted 30’ 0 30’ Hudsonian Hudsonian 350000 101 degrees of thermotectonism during the Paleoproterozoic Trans-Hudson orogeny (Cree Lake Ensialic Mobile by northeasterly structures. The Seal River Domain contains a greater volume of Hudsonian plutons. O 400000 Nunavut O Granite; Gf - pink granite, fluorite bearing; Gj - granite and 0 60 60 0 Granite, massive to foliated, aplite pegmatite; Gp - pink 66 granodiorite diatexite to biotite-metatexite garnet; Zone; Lewry et al., 1978; Lewry and Sibbald, 1980). Parts of the Hearne Province are considered to be H G G Gf W HW 50 porphyritic granite cratonic or semicratonic with respect to the Trans-Hudson Orogen, since they are little affected by Hudsonian The Wollaston Domain is defined by 1) the predominance of supracrustal-derived gneisses of the Wollaston Gw Manitoba Gw - granite and Hurwitz Group metagreywacke, Tk R G 000 thermotectonism. One of these regions, the Ennadai Block (Lewry et al., 1985), trends southwesterly from Group, and 2) the fold-belt structural style. These criteria were first established in Saskatchewan and termed HP P u t a h o w metasiltstone Tn Gj Rankin Inlet to the extreme northwest corner of Manitoba. The Hearne Province is separated from the accreted the Wollaston Fold Belt System (Money, 1965) with a width of approximately 100 km. The Wollaston Domain G Gh Hybrid granite Paleoproterozoic juvenile terranes of the Trans-Hudson Orogen to the south by the Wathaman-Chipewyan in Manitoba is well defined from the Manitoba-Saskatchewan border, where it is approximately 90 km wide Tn Gj T Gh Granite with grey tonalitic to granodioritic gneiss L i t t l e WSk (Whiskey Jack Lake map area, NTS 64K) and trends northeasterly to the south end of Kasmere Lake, where it 000 batholithic domain, which is interpreted as the root of a magmatic arc. HDo T 50 WN Tonalite, cordierite bearing, tourmaline; Tn - tonalite with is approximately 35 km wide (Kasmere Lake map area, NTS 64N). Northeast of Kasmere Lake, the Wollaston HW W 66 Tk WNh Nh T The Ensialic Mobile Zone has been subdivided into six domains in Saskatchewan and Manitoba. They are the Domain is less well defined and narrows to 20 km at the Nunavut border. The Manitoba segment of the G WNk R Quartz feldspar porphyry semipelitic paragneiss to metatexite Mudjatik, Peter Lake (Saskatchewan only), Wollaston, Seal River, Great Island and Nejanilini domains. The Wollaston Domain is characterized by tightly spaced elongate domes, antiforms and synforms that are WNh T T Mudjatik and Wollaston domains and the west end of the Seal River Domain occur in the Kasmere Lake map generally tight to isoclinal. The antiforms contain cores of pelitic and semipelitic gneiss (unit WN) and the WN Wollaston Group HW area (NTS 64N). Tk Tonalite, cordierite bearing tourmaline Meta-arkose; derived arkosic gneiss with metatexite; elongate domes are cored by Archean hypersthene-bearing enderbite to monzocharnockite (unit Zx). The G WSb T T synforms contain in their cores Wollaston Group meta-arkose (unit WSn) or biotite psammite gneiss (unit G Putahow WSn WSb - biotite psammite gneiss, calc-silicate lenses; WSk WSb). WSk - with albite-pyroxene rocks Lithostratigraphy HP Hurwitz Group WNh WNn Metasedimentary rocks of the Paleoproterozoic Hurwitz Group and sedimentary-derived gneissic rocks of the The Seal River Domain occurs east of the Wollaston Domain. It is characterized by large, east to east- WKb Calc-silicate rocks with biotite psammite gneiss Lake Tf HDo Dolomite Wollaston Group unconformably overlie the Archean basement rocks of the Hearne Province. The rocks of the southeast trending folds and faults that have been further deformed by discrete northerly and northeasterly WNh Hurwitz Group occur almost entirely in Nunavut as discontinuous structural keels along a southeasterly trend trending structures. Based on magnetic trends and attitudes of metamorphic layering, the western boundary of Gh WNn Semipelitic paragneiss to metatexite, muscovite cordierite P a r t r i d g e R i v e r NUELTIN LAKE from Rankin Inlet to the northwest corner of Manitoba. the Seal River Domain is irregular and step-like, reflecting a pattern of structural interference. WN garnet sillimanite andalusite hypersthene; W HP Argillite WNj - semipelitic paragneiss to metatexite, + garnet with Tk Tk Kb The west end of the Seal River Domain, for a distance of approximately 40 km to the east, is divided into two Tk WNh granodiorite diatexite to biotite metatexite; WNn - with Hurwitz Group WN WSb segments by the Hudsonian Topp Lake pluton, a large, Paleoproterozoic, synkinematic, porphyritic G tonalite monzogranite intrusion (unit Gp) that occupies the southeast quarter of the Kasmere Lake map area. Tice HW Metagreywacke, metasiltstone Rocks of the Hurwitz Group are present in the northwest corner of the Kasmere Lake map area, based on Tk WN WNn WQ Impure quartzite to quartzite mapping and interpretation by Weber et al. (1975a). Argillite (unit HP) overlain by dolomite (unit HDo) occurs in WNh Southwest of the Topp Lake pluton, the structure is characterized by basin-and-dome polyphase deformation. WSk WNh WNn the Ennadai Block in the extreme northwest of the Kasmere area. The argillite has been correlated with the Wollaston Group This fold pattern is the result of interference of the northeasterly Wollaston fold trend and the easterly Seal Lake T T Ameto Formation of the Hurwitz Group in Nunavut (Weber et al., 1975a) and a metagreywacke, with WNn WSn River fold trend. Major structures are outlined by large-scale layering of supracrustal-derived paragneiss and Biotite psammite gneiss, calc-silicate lenses; WSk - with Proterozoic and/or Archean metasiltstone (unit HW) and minor calc-silicate zones, occurring in the Wollaston Domain from Tice Lake G WSb migmatite. Domes are cored by Archean and/or Hudsonian granitic rocks. The basins are cored by arkosic G albite-pyroxene rocks northeasterly through the area of Putahow Lake into Nunavut. This unit (HW) has been tentatively correlated Foliated alaskite with hybrid granite and pink aplite, gneiss and/or calc-silicate rocks. Synforms in general are highly tightened and the trends of axial traces are G Gk with a similar greywacke of the Hurwitz Group in the Ennadai Lake area (Nunavut). Eade (1971) considered highly variable. This basin-and-dome pattern continues to the southwest into the Whiskey Jack Lake map area WSn Nahili hornblende; Gn - foliated granite the greywacke to be part of the Ameto Formation and possibly time equivalent to the argillite. (NTS 64K). W WK T WK Calc-silicate rocks HDo Sb WN HP G G Granodiorite diatexite to biotite metatexite, garnet Wollaston Group An easterly trending, approximately 40 km wide synform cored by semi-pelitic to pelitic gneiss and intruded by T WNn variably magnetic pink monzogranite, lies on the north flank of the Topp Lake pluton. The south limb of the WK Albite-pyroxene rocks T WSk WK The basal unit of the Wollaston Group in Manitoba and Saskatchewan is a psammitic to semipelitic garnet- synform comprises magnetiferous arkosic gneiss, calc-silicate and biotite psammite gneiss (unit WSb). The Gf WK WNn WSn 0 Tn 0 Archean biotite ± cordierite gneiss (unit WN). It contains sporadic interlayers of calc-silicate rocks and impure to pure north limb of the synform comprises magnetiferous arkosic gneiss, and calc-silicate metasedimentary rocks 45’ R i v e r WSb WQ 45’ Koona Semipelitic paragneiss to metatexite, + garnet; WNn - with quartzite. The gneiss shows a well developed metamorphic layering defined by alternating grey to dark grey, intruded by pyrrhotite-bearing amphibolite after gabbro (Peck et al., 1994). The highly varied magnetic WN tonalite; WNh - with biotite psammite gneiss; WNk - with lits Lake Zx Hypersthene granite (monzocharnokite) biotite-rich layers (1-100 cm thick), and white to cream, medium- to coarse-grained granitic . Both of these signature of the semi-pelitic to pelitic gneiss in the core of the synform is anomalous; regionally, the paragneiss WSn WSb Lake calc-silicate and biotite psammite gneiss HDo WN WK components are intruded by white, pegmatitic, boudinaged sills of granite. Areas underlain by these rocks has a characteristically low magnetic intensity. The magnetic data suggest that the paragneiss may form a thin Tk G WSb Tn coincide with areas of low magnetic intensity (2000-2200 gammas). cover overlying magnetiferous arkosic gneiss. The presence of the basal semi-pelitic to pelitic gneiss in the G G WNn Proterozoic and/or Archean core of the synform overlying younger arkosic gneiss, the uppermost unit of the Wollaston Group, is evidence Tn WK WNn Garnet and cordierite are common accessory minerals in the garnet-biotite gneiss; sillimanite is a minor T of a structural inversion. WNn Granodiorite diatexite to biotite metatexite, garnet component and occurrences of hypersthene and andalusite are more localized (Schledewitz, 1986).
Recommended publications
  • Laurentide Ice-Flow Patterns: a Historical Review, and Implications of the Dispersal of Belcher Islands Erratics"

    Laurentide Ice-Flow Patterns: a Historical Review, and Implications of the Dispersal of Belcher Islands Erratics"

    Article "Laurentide Ice-Flow Patterns: A Historical Review, and Implications of the Dispersal of Belcher Islands Erratics" Victor K. Prest Géographie physique et Quaternaire, vol. 44, n° 2, 1990, p. 113-136. Pour citer cet article, utiliser l'information suivante : URI: http://id.erudit.org/iderudit/032812ar DOI: 10.7202/032812ar Note : les règles d'écriture des références bibliographiques peuvent varier selon les différents domaines du savoir. Ce document est protégé par la loi sur le droit d'auteur. L'utilisation des services d'Érudit (y compris la reproduction) est assujettie à sa politique d'utilisation que vous pouvez consulter à l'URI https://apropos.erudit.org/fr/usagers/politique-dutilisation/ Érudit est un consortium interuniversitaire sans but lucratif composé de l'Université de Montréal, l'Université Laval et l'Université du Québec à Montréal. Il a pour mission la promotion et la valorisation de la recherche. Érudit offre des services d'édition numérique de documents scientifiques depuis 1998. Pour communiquer avec les responsables d'Érudit : [email protected] Document téléchargé le 12 février 2017 05:36 Géographie physique et Quaternaire, 1990, vol. 44, n°2, p. 113-136, 29 fig., 1 tabl LAURENTIDE ICE-FLOW PATTERNS A HISTORIAL REVIEW, AND IMPLICATIONS OF THE DISPERSAL OF BELCHER ISLAND ERRATICS Victor K. PREST, Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8. ABSTRACT This paper deals with the evo­ Archean upland. Similar erratics are common en se fondant sur la croissance glaciaire vers lution of ideas concerning the configuration of in northern Manitoba in the zone of confluence l'ouest à partir du Québec-Labrador.
  • An Overview of World-Class Gold Districts in Canada's Newest

    An Overview of World-Class Gold Districts in Canada's Newest

    JULY 2002 Issue 74 An Overview of World-Class Gold Districts in Canada’s Newest Territory – Nunavut Rob Carpenter Indian and Northern Affairs Canada PO Box 100, Iqaluit, Nunavut, X0A 0H0 Email [email protected] Introduction The Lupin Mine is currently Nunavut’s sole gold producer and has poured over 3 million ounces of bullion since production began in 1982 (Fig. 1). However, recent gold exploration activities across Nunavut have resulted in several significant discov- eries which are at, or approaching, feasibil- ity. This renewed interest in gold explora- tion in Canada’s north is largely due to the availability of extensive, under-explored land parcels that are capable of hosting near-surface and high-grade gold deposits. Acquiring these large land parcels also im- proves the overall effectiveness of explora- tion and increases the chance of discover- ing much sought after gold “districts”, such as the well known Timmins and Kirkland Lake gold districts of the Archean Superior Province. Emerging gold districts in Nunavut in- clude: the Hope Bay Project, located in the northern part of the Archean Slave Prov- ince; the Meadowbank Project, and; the Meliadine Project, both located in the Ar- chean Western Churchill Province (Fig. 1). These districts contain a total gold resource ,QVLGH WKLV LVVXH Fig. 1 – Generalized geology map of Nunavut showing the location of the producing President’s Message 3 Lupin Mine and the Hope Bay, Meadowbank, and Meliadine gold districts as well as other advanced gold exploration projects in the Archean Slave and Western Churchill Duncan Derry Medallist 11 Provinces (after Wheeler et al., 1997).
  • Churchill Wild

    Churchill Wild

    CHURCHILL WILD The World’s NexT GREAT SAFARITM TABLE OF CONTENTS Introduction to Churchill Wild 03 Bird, Bears and Belugas 06 Arctic Discovery 08 Hudson Bay Odyssey 10 Summer Dual Lodge Safari 12 Arctic Safari 14 Fall Dual Lodge Safari 16 Polar Bear Photo Safari - Seal River Heritage Lodge 18 - Nanuk Polar Bear Lodge 20 Great Ice Bear Adventure 22 The Wildest Place on Earth If you’ve ever dreamt of flying over the spectacular Arctic tundra to a remote lodge, walking the Hudson Bay coastline in small groups to view polar bears, and returning to your lodge to unwind by a fireplace before dining on delicious fare…Churchill Wild is your dream come true. Here, among the wilds of northern Manitoba you’ll find diversity of wildlife, the brilliance of the northern lights, and stunning vistas. Each of the safaris in our portfolio is designed to delight your senses and take you on a profound and unforgettable journey into the Arctic wilderness. © Robert Postma © Dennis Fast © Didrik Johnck © Jad Davenport Here’s what truly sets CHURCHILL WILD apart : Canada’s Most Exclusive Polar Bear EcoLodges your experience. With over 100 years of Arctic travel experience in the family, no one knows • Churchill Wild is the only company on the the Hudson Bay coast and surrounding regions planet specializing in ground level walking like we do. tours through the polar bear inhabited remote regions of Arctic Canada. We provide • Beyond incredible polar bears we have access that presents wildlife enthusiasts and exclusive areas for other wildlife viewing photographers with the opportunity of a including beluga whales, wolves, moose, black lifetime amid these stars of the Arctic.
  • Geophysical and Geological Integration and Interpretation of the Northeast Thelon Basin, Nunavut

    Geophysical and Geological Integration and Interpretation of the Northeast Thelon Basin, Nunavut

    GEOPHYSICAL INTERPRETATION OF THE NORTHEAST THELON BASIN GEOPHYSICAL AND GEOLOGICAL INTEGRATION AND INTERPRETATION OF THE NORTHEAST THELON BASIN, NUNAVUT By VICTORIA LYNN TSCHIRHART, B.Sc. A Thesis Submitted to the School of Graduate Studies in Partial Fulfillment of the Requirements for the Degree of Doctorate of Philosophy McMaster University © Copyright for Victoria Tschirhart, November 2013 i McMaster University DOCTORATE OF PHILOSPHY (2013) Hamilton, Ontario TITLE: Geophysical and geological integration and interpretation of the northeast Thelon Basin, Nunavut AUTHOR: Victoria Lynn Tschirhart, B.Sc. (McMaster University) SUPERVISOR: Dr. William A. Morris NUMBER OF PAGES: xii, 196 ii Abstract The northeast Thelon Basin, Nunavut, is a rapidly developing albeit poorly studied, frontier exploration domain for unconformity-associated uranium deposits. Critical criteria for unconformity –associated uranium deposit models are knowledge of the basement geology, fault history and depth to unconformity surface. This thesis sets forth to derive working geological and geophysical models for the northeast Thelon Basin through the implementation of integrated geophysical techniques. A physical rock property database is compiled defining average density and susceptibility values for key map units for integration into subsequent modelling iterations. Forward and inverse potential field modelling using these petrophysical with geological controls define the structure and geometry of the Shultz Lake intrusive complex and northeast Amer Belt, both of which are present below the Thelon sedimentary cover. Implementation of a new source edge detection technique estimates fault development and location within the basin. This provides a quantitative analysis of fault timing, identifying potentially reactivated faults which have an increased likelihood to serve as conduits to transport uranium-rich fluids and focus deposition.
  • The Cultural Ecology of the Chipewyan / by Donald Stewart Mackay.

    The Cultural Ecology of the Chipewyan / by Donald Stewart Mackay.

    ThE CULTURAL ECOLOGY OF TkE CBIPE%YAN UONALD STEhAkT MACKAY b.A., University of british Columbia, 1965 A ThESIS SUBMITTED IN PAhTIAL FULFILLMENT OF THE HEObIRCMENTS FOR THE DEGREE OF MASTER OF ARTS in the department of Sociology and Anthropology @ EONALD STECART MACKAY, 1978 SIMON F hAShR UNlVERSITY January 1978 All rights reserved. This thesis may not be reproduced in whole or in, part, by photocopy or other means, without permission of the author. APPROVAL Name : Donald Stewart Mackay Degree: Master of Arts Title of Thesis: The Cultural Ecology of the Chipewyan Examining Cormnit tee : Chairman : H. Sharp Senior Supervisor- - N. Dyck C.B. Crampton . Fisher Departme'nt of Biological Sciences / ,y/y 1 :, Date Approved: //!,, 1 U The of -- Cultural Ecology .- --------the Chipewyan ----- .- ---A <*PI-: (sign-ir ~re) - Donald Stewart Mackay --- (na~t) March 14, 1978. (date ) AESTRACT This study is concerned with the persistence of human life on the edge of the Canadian Barren Grounds. The Chipewyan make up the largest distinct linguistic and cultural group and are the most easterly among the Northern Athapaskan Indians, or Dene. Over many centuries, the Chipewyan have maintained a form of social life as an edge-of-the-forest people and people of the Barren Grounds to the west of Hudson Bay. The particular aim of this thesis is to attempt, through a survey of the ecological and historical 1iterature , to elucidate something of the traditional adaptive pattern of the Chipewyan in their explcitation of the subarc tic envirorient . Given the fragmentary nature of much of the historical evidence, our limited understanding of the subarctic environment, and the fact that the Chipewyan oecumene (way of looking at life) is largely denied to the modern observer, we acknowledge that this exercise in ecological and historical reconstruction is governed by serious hazards and limitations.
  • Technical Report on the Gold and Base Metal Potential of the Sy Property, Nunavut, Canada

    Technical Report on the Gold and Base Metal Potential of the Sy Property, Nunavut, Canada

    NTS 65 I/04 to I/06 and J/01 TECHNICAL REPORT ON THE GOLD AND BASE METAL POTENTIAL OF THE SY PROPERTY, NUNAVUT, CANADA Completed By: APEX Geoscience Ltd. Suite 200, 9797-45 Avenue Edmonton, Alberta, Canada T6E 5V8 Completed For: Corsa Capital Ltd. Suite 1440, 625 Howe Street Vancouver, BC V6C 2T6 December 4th, 2007 M.B. Dufresne, M.Sc., P.Geol. TECHNICAL REPORT ON THE GOLD AND BASE METAL POTENTIAL OF THE SY PROPERTY, NUNAVUT, CANADA TABLE OF CONTENTS PAGE SUMMARY...................................................................................................................... 1 INTRODUCTION AND TERMS OF REFERENCE.......................................................... 3 RELIANCE ON OTHER EXPERTS................................................................................. 3 PROPERTY LOCATION AND DESCRIPTION ............................................................... 4 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY............................................................................................................ 8 HISTORY ........................................................................................................................ 8 GEOLOGICAL SETTING .............................................................................................. 15 Regional Geology ............................................................................................... 15 Property Geology ............................................................................................... 16 DEPOSIT
  • Canarc Resource Corp. Hard Cash Project Summary

    Canarc Resource Corp. Hard Cash Project Summary

    CANARC RESOURCE CORP. T: 604.685.9700 www.canarc.net Suite 810 – 625 Howe Street F: 604.685.9744 CCM: TSX Vancouver, BC V6C 2T6 TF: 1.877.684.9700 CRCUF: OTCQX Canarc Resource Corp. Hard Cash Project Summary Canarc Resource Corp. ( Canarc ) is a Vancouver based gold exploration company with a number of projects in Nevada and British Columbia as well as the Hard Cash and Nigel properties in Nunavut. The Hard Cash property, consisting of Claims RLN 3-4 (K14329-30) covering 2,090 hectares on Crown Land, is located in the Ennadai Greenstone Belt in SW Nunavut on the shores of Ennadai Lake. The property is 405 km from Arviat, Nunavut, 310 km NE of Stony Rapids, Saskatchewan and is accessible by float plane or helicopter. There is an all-weather gravel airstrip at Ennadai Lake Lodge which is owned by Arctic Haven, 22 kms southwest of the property. Mineralization on the property was previously discovered by Don Cameron in 1946 at the Swamp Showing. The showing was staked and 9 shallow holes were drilled and several blast trenches excavated at the northern end of the Swamp Showing near Ennadai Lake. Giant Yellowknife Mines acquired the property in 1981 and took a claim to lease. Phelps Dodge optioned the lease and staked the surrounding area in 1995 and conducted surface exploration from 1995 to 1997. The claims were allowed to lapse and were re-staked by Panarc Resources in January 2011. In 2012, Panarc conducted prospecting and geological mapping focused on the Swamp Showing. The claims were subsequently sold to Silver Range Resources Ltd.
  • PROVINCIAL GOVERNMENTS 9.—Provinces and Territories Of

    PROVINCIAL GOVERNMENTS 9.—Provinces and Territories Of

    PROVINCIAL GOVERNMENTS 83 9.—Provinces and Territories of Canada, with present Areas, Dates of Admission to Confederation and Legislative Process by which this was effected. Present Area (square miles). Province, Date of Territory Admission Legislative Process. or District. or Creation. Land. Water. Total. Ontario July 1, 1867[Ac t of Imperial Parliament—The] 357,962 49,300 407,2621 Quebec " 1, 1867J British North America Act, 18671 571,004 23,430 594,4342 Nova Scotia " 1, 1867 (30-31 Vict., c. 3), and Imperial! 20,743 685 21,428 New Brunswick.. " 1, 1867[ Order in Council of May 22,1867. J 27,710 275 27,985 Manitoba " 15, 1870Manitob a Act, 1870 (33 Vict., c. 3) and Imperial Order in Council, June 23, 1870 224,777 27,055 251,8323 British Columbia. " 20, 1871Imperia l Order in Council, May 16,1871 349,970 5,885 355,855 P.E. Island " 1, 1873Imperia l Order in Council, June 26,1873 2,184 2,184 Saskatchewan Sept. 1, 1905Saskatchewa n Act, 1905 (4-5 Edw. VII, c. 42) 237,975 13,725 251,700* Alberta. " 1, 1905Albert a Act, 1905 (4-5 Edw. VII, c. 3). 248,80J 6,485 255,285* Yukon.. June 13, 1898Yuko n Territory Act, 1898 (61 Vict., c.6) 205,346 1,730 207,076 Mackenzie. Jan. 1, 1920 493,225 34,265 527,490 s Keewatin.. " 1, 1920-Orde r in Council, Mar. 16,1918. 218,460 9,700 228,160s Franklin... " 1, 1920 546,532 7,500 554,0325 Total. 3,504,688 180,035 3,684,733 1 The area of Ontario was extended by the Canada (Ontario Boundary) Act, 1889, and the Ontario Boundaries Extension Act, 1912 (2 Geo.
  • CNGO NU Summary-Of-Activities

    CNGO NU Summary-Of-Activities

    SUMMARY OF ACTIVITIES 2015 © 2015 by Canada-Nunavut Geoscience Office. All rights reserved. Electronic edition published 2015. This publication is also available, free of charge, as colour digital files in Adobe Acrobat® PDF format from the Canada- Nunavut Geoscience Office website: www.cngo.ca/ Every reasonable effort is made to ensure the accuracy of the information contained in this report, but Natural Resources Canada does not assume any liability for errors that may occur. Source references are included in the report and users should verify critical information. When using information from this publication in other publications or presentations, due acknowledgment should be given to Canada-Nunavut Geoscience Office. The recommended reference is included on the title page of each paper. The com- plete volume should be referenced as follows: Canada-Nunavut Geoscience Office (2015): Canada-Nunavut Geoscience Office Summary of Activities 2015; Canada- Nunavut Geoscience Office, 208 p. ISSN 2291-1235 Canada-Nunavut Geoscience Office Summary of Activities (Print) ISSN 2291-1243 Canada-Nunavut Geoscience Office Summary of Activities (Online) Front cover photo: Sean Noble overlooking a glacially eroded valley, standing among middle Paleoproterozoic age psam- mitic metasedimentary rocks, nine kilometres west of Chidliak Bay, southern Baffin Island. Photo by Dustin Liikane, Carleton University. Back cover photo: Iqaluit International Airport under rehabilitation and expansion; the Canada-Nunavut Geoscience Of- fice, Geological Survey of Canada (Natural Resources Canada), Centre d’études nordiques (Université Laval) and Trans- port Canada contributed to a better understanding of permafrost conditions to support the planned repairs and adapt the in- frastructure to new climatic conditions. Photo by Tommy Tremblay, Canada-Nunavut Geoscience Office.
  • Medicine in Manitoba

    Medicine in Manitoba

    Medicine in Manitoba THE STORY OF ITS BEGINNINGS /u; ROSS MITCHELL, M.D. THE UNIVERSITY OF CALGARY LIBRARY FR OM THE ESTATE OF VR. E.P. SCARLETT Medic1'ne in M"nito/J" • THE STORY OF ITS BEGINNINGS By ROSS MITCHELL, M. D. .· - ' TO MY WIFE Whose counsel, encouragement and patience have made this wor~ possible . .· A c.~nowledg ments THE LATE Dr. H. H. Chown, soon after coming to Winnipeg about 1880, began to collect material concerning the early doctors of Manitoba, and many years later read a communication on this subject before the Winnipeg Medical Society. This paper has never been published, but the typescript is preserved in the medical library of the University of Manitoba and this, together with his early notebook, were made avail­ able by him to the present writer, who gratefully acknowledges his indebtedness. The editors of "The Beaver": Mr. Robert Watson, Mr. Douglas Mackay and Mr. Clifford Wilson have procured informa­ tion from the archives of the Hudson's Bay Company in London. Dr. M. T. Macfarland, registrar of the College of Physicians and Surgeons of Manitoba, kindly permitted perusal of the first Register of the College. Dr. J. L. Johnston, Provincial Librarian, has never failed to be helpful, has read the manuscript and made many valuable suggestions. Mr. William Douglas, an authority on the Selkirk Settlers and on Free' masonry has given precise information regarding Alexander Cuddie, John Schultz and on the numbers of Selkirk Settlers driven out from Red River. Sheriff Colin Inkster told of Dr. Turver. Personal communications have been received from many Red River pioneers such as Archbishop S.
  • Gjoa Haven © Nunavut Tourism

    Gjoa Haven © Nunavut Tourism

    NUNAVUT COASTAL RESOURCE INVENTORY ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut Ministère de l’Environnement Gjoa Haven © Nunavut Tourism ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut NUNAVUT COASTAL RESOURCE INVENTORY • Gjoa Haven INVENTORY RESOURCE COASTAL NUNAVUT Ministère de l’Environnement Nunavut Coastal Resource Inventory – Gjoa Haven 2011 Department of Environment Fisheries and Sealing Division Box 1000 Station 1310 Iqaluit, Nunavut, X0A 0H0 GJOA HAVEN Inventory deliverables include: EXECUTIVE SUMMARY • A final report summarizing all of the activities This report is derived from the Hamlet of Gjoa Haven undertaken as part of this project; and represents one component of the Nunavut Coastal Resource Inventory (NCRI). “Coastal inventory”, as used • Provision of the coastal resource inventory in a GIS here, refers to the collection of information on coastal database; resources and activities gained from community interviews, research, reports, maps, and other resources. This data is • Large-format resource inventory maps for the Hamlet presented in a series of maps. of Gjoa Haven, Nunavut; and Coastal resource inventories have been conducted in • Key recommendations on both the use of this study as many jurisdictions throughout Canada, notably along the well as future initiatives. Atlantic and Pacific coasts. These inventories have been used as a means of gathering reliable information on During the course of this project, Gjoa Haven was visited on coastal resources to facilitate their strategic assessment, two occasions:
  • Technical Report on the Mineral Resources and Mineral Reserves at Meadowbank Gold Mine, Nunavut, Canada

    Technical Report on the Mineral Resources and Mineral Reserves at Meadowbank Gold Mine, Nunavut, Canada

    Technical Report on the Mineral Resources and Mineral Reserves at Meadowbank Gold Mine, Nunavut, Canada as at December 31, 2011 NTS 56E/4 and 66H/1, UTM (Zone 14): 638,000 metres East, 7,214,000 metres North PREPARED FOR Agnico-Eagle Mines Limited 145 King Street East, Suite 400 Toronto, Ontario, Canada M5C 2Y7 Telephone: / 416.947.1212 Facsimile: / 416.367.4681 BY Marc Ruel, P.Geo. Alex Proulx, ing. Pathies Nawej Muteb, ing. Larry Connell, P.Eng. February 15, 2012 Date and Signature Page The data on which the contained Mineral Reserve and Mineral Resource estimate for the Meadowbank mine is based were current as of the Effective Date, February 15, 2012. The undersigned are all qualified persons and were responsible for preparing or supervising the preparation of parts of this Technical Report, as described in Item 2. (Signed by) Marc Ruel Date: _March 23, 2012_ Marc Ruel, P.Geo. (Quebec #0365), (sealed) (Signed by) Alexandre Proulx Date: _ March 23, 2012 Alexandre Proulx, ing. (OIQ #117423), (sealed) (Signed by) Pathies Nawej Muteb Date: March 23, 2012_ Pathies Nawej Muteb, ing. (OIQ #144728), (sealed) (Signed by) Larry Connell Date: March 23, 2012_ Larry Connell, P.Eng. (British Columbia #23696, Ontario #9099508, NWT/NU #L1720), (sealed) Contents DATE AND SIGNATURE PAGE .............................................................................................. II ITEM 1. SUMMARY ............................................................................................................. 1 1.1 PROPERTY DESCRIPTION AND LOCATION ..........................................................................